Search results for "Wetted perimeter"

showing 9 items of 9 documents

Flow resistance equation for rills

2017

In this paper, a new flow resistance equation for rill flow was deduced applying dimensional analysis and self‐similarity theory. At first, the incomplete self‐similarity hypothesis was used for establishing the flow velocity distribution whose integration gives the theoretical expression of the Darcy–Weisbach friction factor. Then the deduced theoretical resistance equation was tested by some measurements of flow velocity, water depth, cross section area, wetted perimeter, and bed slope carried out in 106 reaches of some rills shaped on an experimental plot. A relationship between the velocity profile, the channel slope, and the flow Froude number was also established. The analysis showed …

010504 meteorology & atmospheric sciences0208 environmental biotechnology02 engineering and technology01 natural sciencesPlot (graphics)Physics::Fluid Dynamicssymbols.namesakeWetted perimeterFroude numberSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliGeotechnical engineering0105 earth and related environmental sciencesWater Science and TechnologyFlow resistancegeographysoil erosiongeography.geographical_feature_categoryrill flowMechanicsplot measurement020801 environmental engineeringRillDistribution (mathematics)Flow resistanceFlow velocityFlow (mathematics)velocity profilesymbolsGeologyHydrological Processes
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Testing a theoretical resistance law for overland flow on a stony hillslope

2020

Overland flow, sediments, and nutrients transported in runoff are important processes involved in soil erosion and water pollution. Modelling transport of sediments and chemicals requires accurate estimates of hydraulic resistance, which is one of the key variables characterizing runoff water depth and velocity. In this paper, a new theoretical power–velocity profile, originally deduced neglecting the impact effect of rainfall, was initially modified for taking into account the effect of rainfall intensity. Then a theoretical flow resistance law was obtained by integration of the new flow velocity distribution. This flow resistance law was tested using field measurements by Nearing for the …

010504 meteorology & atmospheric sciencesFlow (psychology)rainfall0207 environmental engineering02 engineering and technology01 natural sciencessymbols.namesakeWetted perimeteroverland flowdimensional analysiFroude numberSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestali020701 environmental engineering0105 earth and related environmental sciencesWater Science and Technologyself-similarityReynolds numberLaminar flowstony hillslopeFlow velocityLawsymbolsvelocity profileEnvironmental scienceSurface runoffflow resistanceIntensity (heat transfer)
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Comparing flow resistance law for fixed and mobile bed rills

2019

Rills caused by run-off concentration on erodible hillslopes have very irregular profiles and cross-section shapes. Rill erosion directly depends on the hydraulics of flow in the rills, which may differ greatly from hydraulics of flow in larger and regular channels. In this paper, a recently theoretically deduced rill flow resistance equation, based on a power–velocity profile, was tested experimentally on plots of varying slopes (ranging from 9% to 26%) in which mobile and fixed bed rills were incised. Initially, measurements of flow velocity, water depth, cross-section area, wetted perimeter, and bed slope, carried out in 320 reaches of mobile bed rills and in 165 reaches of fixed rills, …

010504 meteorology & atmospheric sciencesHydraulicsfixed bedFlow (psychology)0207 environmental engineering02 engineering and technology01 natural scienceslaw.inventionWetted perimetersymbols.namesakelawFroude numberSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestalirill hydraulic020701 environmental engineering0105 earth and related environmental sciencesWater Science and Technologygeographysoil erosiongeography.geographical_feature_categoryrill flowplot measurementRillFlow conditionsFlow velocitymobile bedsymbolsflow resistanceSediment transportGeologyHydrological Processes
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Testing a theoretical resistance law for overland flow under simulated rainfall with different types of vegetation

2020

Abstract In this paper a recently theoretically deduced flow resistance equation, based on a power-velocity profile, was tested using data collected for overland flow under simulated rainfall carried out in plots with vegetation. The available data were obtained exploring a wide range of rainfall intensities (from 60 to 181 mm h−1) and slopes (from 3.6 to 39.6%), and with four different types of vegetation. The database, including measurements of flow velocity, water depth, cross sectional flow area, wetted perimeter and bed slope, was divided in four datasets (one for each vegetation type), which allowed the calibration of the relationship between the velocity profile parameter Γ, the slop…

Dimensional analysi010504 meteorology & atmospheric sciencesSoil science01 natural sciencessymbols.namesakeWetted perimeterVelocity profileFroude numbermedicineSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliVegetable cover0105 earth and related environmental sciencesEarth-Surface ProcessesReynolds numberLaminar flow04 agricultural and veterinary sciencesOpen channel flowOpen-channel flowSelf-similarityFlow (mathematics)Flow velocityFlow resistance040103 agronomy & agriculturesymbolsRainfall simulationSoil erosion0401 agriculture forestry and fisheriesEnvironmental sciencemedicine.symptomVegetation (pathology)
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Testing a theoretically-based overland flow resistance law by Emmett’s database

2021

Abstract The main aim of this paper was to test a recently theoretically deduced flow resistance equation, based on a power-velocity profile, using a wide database of available measurements carried out in laboratory and field experimental runs with overland flow under simulated rainfall. In comparison with previous calibrations and validations of this theoretically deduced flow resistance equation, the used database by Emmett is characterized by a wide range of rainfall intensities (from 79.2 to 303.5 mm h−1 for laboratory runs and from 178.3 to 215.9 mm h−1 for field investigations) and bed slopes (from 0.33 to 17% for laboratory runs and from 2.9 to 33.2% for field investigations). For th…

Dimensional analysiVegetationDatabaseReynolds numberLaminar flowcomputer.software_genreSelf-similaritysymbols.namesakeWetted perimeterOverland flowVelocity profileFlow (mathematics)Flow velocityLawRainfall simulationFroude numbersymbolsSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliEnvironmental scienceSurface runoffcomputerIntensity (heat transfer)Water Science and TechnologyJournal of Hydrology
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Estimación mediante programación genética de los patrones del suelo humectantes para el riego por goteo

2012

Drip irrigation is considered as one of the most efficient irrigation systems. Knowledge of the soil wetted perimeter arising from infiltration of water from drippers is important in the design and management of efficient irrigation systems. To this aim, numerical models can represent a powerful tool to analyze the evolution of the wetting pattern during irrigation, in order to explore drip irrigation management strategies, to set up the duration of irrigation, and finally to optimize water use efficiency. This paper examines the potential of genetic programming (GP) in simulating wetting patterns of drip irrigation. First by considering 12 different soil textures of USDA–SCS soil texture t…

Hydrologysoil texture triangleIrrigationHydrusnumerical modelsinfiltraciónSoil textureHYDRUS 2Dmodelos numéricosDrip irrigationinfiltrationtriángulo de texturas del suelosoil texture triangle.Wetted perimeterInfiltration (hydrology)LoamSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestaligenetic programmingprogramación genéticaWettingnumerical modelAgronomy and Crop ScienceMathematics
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Flow resistance law under suspended sediment laden conditions

2020

Abstract The uniform flow resistance equation, in the form due to Manning or Darcy-Weisbach, is widely applied to establish the stage-discharge relationship of a river cross-section. The application of this equation, namely the slope-area method, allows to indirectly measure the corresponding river discharge by measurements of bed slope, water level, cross-section area, wetted perimeter and an estimate of channel roughness. In this paper, a recently deduced flow resistance equation for open channel flow was tested during conditions of suspended sediment-laden flow. First, the flow resistance equation was determined by dimensional analysis and by applying the condition of incomplete self-sim…

Materials science0207 environmental engineeringSediment02 engineering and technologyMechanicsDimensional analysis Flow resistance Flow velocity profile Self-similarity Suspended-load01 natural sciencesComputer Science ApplicationsOpen-channel flow010309 opticssymbols.namesakeWetted perimeterFlow conditionsFlow velocityFlow (mathematics)Modeling and Simulation0103 physical sciencesFroude numbersymbolsSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliPotential flowElectrical and Electronic Engineering020701 environmental engineeringInstrumentationFlow Measurement and Instrumentation
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Flow resistance of overland flow on a smooth bed under simulated rainfall

2020

In this paper a recently theoretically deduced flow resistance equation, based on a power-velocity profile, was tested using laboratory measurements by Yoon and Wenzel for an overland flow on a smooth bed under rainfall. These measurements of the Darcy-Weisbach friction factor, corresponding to a wide range of the flow Reynolds number (191–5700), were carried out for an overland flow under a simulated rainfall characterized by different intensity values ranging from 13 to 381 mm h−1. At first, the available measured values of flow velocity, water depth, cross sectional area, wetted perimeter and bed slope were used to calibrate the relationship between the velocity profile parameter Γ, the …

RainfallDimensional analysi010504 meteorology & atmospheric sciencesFlow (psychology)01 natural sciencessymbols.namesakeWetted perimeterOverland flowVelocity profileFroude numberRange (statistics)Settore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestali0105 earth and related environmental sciencesEarth-Surface ProcessesTurbulenceReynolds number04 agricultural and veterinary sciencesMechanicsSelf-similarityFlow velocityFlow resistance040103 agronomy & agriculturesymbols0401 agriculture forestry and fisheriesGeologyIntensity (heat transfer)
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Experiments for testing soil texture effects on flow resistance in mobile bed rills

2018

Abstract In this paper a recently theoretically deduced rill flow resistance equation, based on a power-velocity profile, was tested experimentally on plots of varying slopes and soil texture in which mobile bed rills are incised. Measurements of flow velocity, water depth, cross section area, wetted perimeter and bed slope conducted in rill reaches incised on experimental plots, having different slope values (9, 14, 22, 24 and 26%) and soil texture (clay fraction ranging from 42 to 73%), and literature data were used to calibrate the flow resistance equation. In particular, the relationship between the velocity profile parameter Γ, the channel slope, the flow Froude number and texture frac…

geographygeography.geographical_feature_categorySoil textureRill hydraulic0208 environmental biotechnologyFlow (psychology)Soil science02 engineering and technologyPlot measurement020801 environmental engineeringRillWetted perimetersymbols.namesakeVelocity profileFlow resistanceFlow velocitySoil textureSoil waterSoil erosionFroude numbersymbolsSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliTexture (crystalline)GeologyEarth-Surface ProcessesCATENA
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